Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals)
Mineralogical composition features of large copper-pyritic Yubileinoye deposit (slightly metamorphized and now exploited by open pit) are studied. Major ore structures include impregnated, spotted, banded, stringer structures. Two generations of chalcopyrite, sphalerite and quartz, and 3 generation...
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Format: | Article |
Language: | English |
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Peoples’ Friendship University of Russia (RUDN University)
2011-03-01
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Series: | RUDN Journal of Engineering Research |
Subjects: | |
Online Access: | http://journals.rudn.ru/engineering-researches/article/view/4781 |
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author | I V Vikentyev A G Saenko E V Karelina A I Ezhov N V Trubkin |
author_facet | I V Vikentyev A G Saenko E V Karelina A I Ezhov N V Trubkin |
author_sort | I V Vikentyev |
collection | DOAJ |
description | Mineralogical composition features of large copper-pyritic Yubileinoye deposit (slightly metamorphized and now exploited by open pit) are studied. Major ore structures include impregnated, spotted, banded, stringer structures. Two generations of chalcopyrite, sphalerite and quartz, and 3 generation of pyrite were found. Proper gold minerals occur as tiny isolations of native gold (fineness 631-662) in veinlets accompanied by tennantite-tetrahedrite and galena; the connection of native gold with these minerals is supported by close correlation Au with Pb, As and Sb in ore composition. |
first_indexed | 2024-03-12T07:42:48Z |
format | Article |
id | doaj.art-98aea20ba7884cf4a0a101e2ba46fdc8 |
institution | Directory Open Access Journal |
issn | 2312-8143 2312-8151 |
language | English |
last_indexed | 2024-03-12T07:42:48Z |
publishDate | 2011-03-01 |
publisher | Peoples’ Friendship University of Russia (RUDN University) |
record_format | Article |
series | RUDN Journal of Engineering Research |
spelling | doaj.art-98aea20ba7884cf4a0a101e2ba46fdc82023-09-02T21:11:58ZengPeoples’ Friendship University of Russia (RUDN University)RUDN Journal of Engineering Research2312-81432312-81512011-03-010184904781Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals)I V Vikentyev0A G Saenko1E V Karelina2A I Ezhov3N V Trubkin4Российский университет дружбы народовРоссийский университет дружбы народовРоссийский университет дружбы народовРоссийский университет дружбы народовИГЕМ РАНMineralogical composition features of large copper-pyritic Yubileinoye deposit (slightly metamorphized and now exploited by open pit) are studied. Major ore structures include impregnated, spotted, banded, stringer structures. Two generations of chalcopyrite, sphalerite and quartz, and 3 generation of pyrite were found. Proper gold minerals occur as tiny isolations of native gold (fineness 631-662) in veinlets accompanied by tennantite-tetrahedrite and galena; the connection of native gold with these minerals is supported by close correlation Au with Pb, As and Sb in ore composition.http://journals.rudn.ru/engineering-researches/article/view/4781Южный Уралколчеданная рудаструктуратекстурасульфидыпиритсамородное золото |
spellingShingle | I V Vikentyev A G Saenko E V Karelina A I Ezhov N V Trubkin Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) RUDN Journal of Engineering Research Южный Урал колчеданная руда структура текстура сульфиды пирит самородное золото |
title | Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) |
title_full | Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) |
title_fullStr | Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) |
title_full_unstemmed | Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) |
title_short | Mineralogical features of ore of copper-pyritic deposit Yubileinoye (S. Urals) |
title_sort | mineralogical features of ore of copper pyritic deposit yubileinoye s urals |
topic | Южный Урал колчеданная руда структура текстура сульфиды пирит самородное золото |
url | http://journals.rudn.ru/engineering-researches/article/view/4781 |
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